Justin P Dodd
Datos Biográficos
| ID | 843089 |
|---|---|
| NOMBRE | Justin P Dodd |
| NOMBRES | Justin P |
| APELLIDO | Dodd |
| FIRMA | DODD J P |
| AFILIACIONES | Northern Illinois University |
| ORCID | 0000-0002-2964-3566 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 4 |
| TOTAL DE CITAS | 2 |
| TOTAL COMO AUTOR | 4 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 2013 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2022 |
| ÍNDICE H | 1 |
A Late Holocene Stable Isotope and Carbon Accumulation Record from Teringi Bog in Southern Estonia
Radiocarbon-dated peat cores collected from an ombrotrophic bog in southern Estonia record shifting environmental conditions and carbon accumulation rates in northern Europe during the late Holocene. Modern observations indicate that the water balance of the peatland is highly influenced by changes in relative humidity, followed by temperature and precipitation. The modern δ18O and δ2H values of surface water suggest that the groundwater is an in…
Mid‐Holocene environmental change and human occupation at Sai Island, Northern Sudan
Holocene environmental change in the northern and central Nile Valley was controlled primarily by shifts in the Intertropical Convergence Zone over time, leading to changes in aridity and water availability for early occupants of the region. Although local environmental changes may help to motivate societal changes such as those in settlement patterns or technological productions, evidence from pedogenic carbonates at Sai Island, in northern Suda…
Overview of the oxygen isotope systematics of land snails from North America
Continental paleoclimate proxies with near-global coverage are rare. Land snail δ 18 O is one of the few proxies abundant in Quaternary sediments ranging from the tropics to the high Arctic tundra. However, its application in paleoclimatology remains difficult, attributable in part to limitations in published calibration studies. Here we present shell δ 18 O of modern small ( 18 O at a coarse scale. This transect is augmented by published δ 18 O …
Domesticando El Desierto
The deserT. environmenT and human
Mid‐Holocene environmental change and human occupation at Sai Island, Northern Sudan
Holocene environmental change in the northern and central Nile Valley was controlled primarily by shifts in the Intertropical Convergence Zone over time, leading to changes in aridity and water availability for early occupants of the region. Although local environmental changes may help to motivate societal changes such as those in settlement patterns or technological productions, evidence from pedogenic carbonates at Sai Island, in northern Suda…
Domesticando El Desierto
The deserT. environmenT and human
Domesticando El Desierto
The deserT. environmenT and human
Overview of the oxygen isotope systematics of land snails from North America
Continental paleoclimate proxies with near-global coverage are rare. Land snail δ 18 O is one of the few proxies abundant in Quaternary sediments ranging from the tropics to the high Arctic tundra. However, its application in paleoclimatology remains difficult, attributable in part to limitations in published calibration studies. Here we present shell δ 18 O of modern small ( 18 O at a coarse scale. This transect is augmented by published δ 18 O …
Mid‐Holocene environmental change and human occupation at Sai Island, Northern Sudan
Holocene environmental change in the northern and central Nile Valley was controlled primarily by shifts in the Intertropical Convergence Zone over time, leading to changes in aridity and water availability for early occupants of the region. Although local environmental changes may help to motivate societal changes such as those in settlement patterns or technological productions, evidence from pedogenic carbonates at Sai Island, in northern Suda…
A Late Holocene Stable Isotope and Carbon Accumulation Record from Teringi Bog in Southern Estonia
Radiocarbon-dated peat cores collected from an ombrotrophic bog in southern Estonia record shifting environmental conditions and carbon accumulation rates in northern Europe during the late Holocene. Modern observations indicate that the water balance of the peatland is highly influenced by changes in relative humidity, followed by temperature and precipitation. The modern δ18O and δ2H values of surface water suggest that the groundwater is an in…
Geography (4 obras) · Geology and Paleoclimatology Research (3 obras) · Archaeology (2 obras) · Archaeology and ancient environmental studies (2 obras) · Arid (2 obras) · Biology (2 obras) · Climate change (2 obras) · Holocene (2 obras) · Physical geography (2 obras) · Precipitation (2 obras)